2019-01-21T21:36:35Zhttp://doidb.wdc-terra.org/oaip/oaioai:doidb.wdc-terra.org:10002016-11-25T14:16:14ZDOIDBDOIDB.SDDB10.1594/GFZ.SDDB.1408Thermal Conductivity of Cores of the KTB Main Hole HB1 (measured data)KTB, WG GeophysicsThermal Conductivity of Cores of the KTB Main Hole HB1 (measured data)2010-09-29Potsdam, GermanyDeutsches GeoForschungsZentrum GFZDatasethttp://dx.doi.org/10.1594/GFZ.SDDB.1408Earth ScienceEARTH SCIENCESolid EarthRocks/MineralsMinerals/CrystalsEARTH SCIENCESolid EarthDeep DrillingWell-LoggingAnisotropy of thermal conductivityDate of SamplingThermal Conductivity, maxThermal Conductivity, max angleThermal Conductivity, meanThermal Conductivity, mincalculationLand basedComplete49.58849.58812.19212.192KTBGerman Continental Deep Drilling ProgramBMBFBundesministerium für Bildung und Forschungcc-byEnglishSDDBScientific Drilling Databasehttp://www.scientificdrilling.orgDATA CENTER CONTACT###DC_PERSONNEL_LAST###Online Internet (HTTP)The thermal conductivity on cores is measured in two steps (see Pribnow 1994). First, one face end of the core is sawed and polished. The half space line source is pressed against this preparated face (without further contact medium like water) by a computerized device. The position of the heat source is varied in 15 degree intervals around one semicircle. At each position, 3 repeating measurements are performed. The line source azimuth of the lowest measured thermal conductivity is the strike of the foliation plane. On the other hand, the thermal conductivity is maximal parallel to that direction. This apparent paradox can be explained by the experimental method, because the measurement plane is perpendicular to the orientation of the line source (Pribnow 1994).In a second step a calotte plane perpendicular to the strike of foliation is prepared. A second series of thermal conductivity measurements in 15 degree intervals ...CEOS IDN DIF9.7